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An unusual diagenetic structure in the Precambrian banded iron formation (BIF) of Orissa, India, and its interpretation

✍ Scribed by K. L. Chakraborty; T. Majumder


Publisher
Springer
Year
1992
Tongue
English
Weight
716 KB
Volume
27
Category
Article
ISSN
0026-4598

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✦ Synopsis


An unusual type of late diagenetic tectonic and compaction structure simulating boudinage phenomena is described and documented from the Precambrian banded iron formation (BIF) of Orissa, India. The structure was seemingly initiated by the development of tension cracks in the hydroplastic stage followed by rotation and imbrication of the segments of the iron (magnetite) bands. The tension cracks were subsequently filled up by finely crystalline diagenetic quartz veins.